Potential Role of Feldspathic Sandstone as a Natural Water Retaining Agent in Mu Us Sandy Land, Northwest China

Key words: 
• feldspathic sandstone /
• sandy land soil /
• water retaining agent /
• Mu Us Sandy Land /
• soil saturatd hydraulic conductivity

Abstract: This paper analyzed the water-retention mechanism of feldspathic sandstone (fine- (< 1 mm diam.) and gravel-sized (2–3 cm
diam.) in Mu Us Sandy Land, Northwest China. The objective of this study is to study the effect of feldspathic sandstone amendment on
water retention in sandy land. The results showed that as the proportion of fine  feldspathic sandstone in the sandy land soil increased,
the soil texture changed from sand to silt loam, the capillary porosity gradually increased from 26.3% to 44.9%, and the soil saturated
hydraulic conductivity decreased from 7.10 mm/min to 0.07 mm/min. Feldspathic sandstone gravel formed micro-reservoirs in the sandy
land soil, playing the role of a ′water absorbent′ and ′water retaining agent′ in sandy land. Amendment with feldspathic sandstone can
increase water retention in the arable layer of sandy land by 67%. This study provides a theoretical basis for the amelioration of sandy
land on a large scale. It can be concluded that amendment with feldspathic sandstone can improve the physical properties of sandy land
soil and increase soil water retention.